Geological characteristics and origin of the Hadamengou gold deposit in Inner Mongolia, China

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• 作者：Yu Zhang ; Jianchao Liu ; Haidong Zhang ; Shaopeng Zhang
• 关键词：Hadamengou gold deposit ; Wulashan Group ; Northern margin of the North China Craton ; Gold mineralization
• 刊名：Arabian Journal of Geosciences
• 出版年：2016
• 出版时间：April 2016
• 年：2016
• 卷：9
• 期：4
• 全文大小：1,802 KB
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• 作者单位：Yu Zhang (1)
  Jianchao Liu (1)
  Haidong Zhang (1)
  Shaopeng Zhang (2)
  
  1. The School of Earth Science and Resources, Chang’an University, Xi’an, 710054, China
  2. Remote Sensing Application Institute, Aerophotogrammetry and Remote Sensing Bureau, Xi’an, 710054, China
  
• 刊物类别：Earth and Environmental Science
• 出版者：Springer Berlin Heidelberg
• ISSN：1866-7538

文摘

The Hadamengou gold deposit is located in the western segment of the northern margin of the North China Craton (NCC). It is hosted by Archean metamorphic rocks of the Wulashan Group. The main ore types include gold-bearing quartz vein type, gold-bearing quartz-potassic feldspar vein type, and gold-bearing altered rock type. Gold mineralization is closely related to K-feldspathization. Hydrogen and oxygen isotope data indicate that ore-forming fluids were dominated by magmatic water mixed with minor meteoric water. Sulfur and lead isotope data indicate that metallogenic materials were mainly supplied by the magmatic and Archean Wulashan Group. The gold mineralization was mainly formed during the Early Indosinian tectonic movement, which drove ore-forming fluids to the favorable depositional environment. The northern margin of the NCC is a prospective area for gold exploration. Gold deposits hosted by or related to alkaline intrusions have become one of the most important mineral exploration targets in northern China.